Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266

The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal that is traceable in deep-sea cores taken in high latitude regions of the Southern hemisphere. This signal may be weakened by noise due to (1) terrestrially derived debris in areas close to the continents; (2) changing...

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Bibliographic Details
Main Author: Sackett, William M
Format: Dataset
Language:English
Published: PANGAEA 1986
Subjects:
28-266
Antarctic Ocean/RIDGE
Calcium carbonate
Carbon
organic
total
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Epoch
Glomar Challenger
Leg28
Sample code/label
δ13C
organic carbon
Antarctic
Antarctic Ocean
Antarc*
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.757317
https://doi.org/10.1594/PANGAEA.757317
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.757317
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.757317 2023-05-15T13:41:33+02:00 Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266 Sackett, William M LATITUDE: -56.402200 * LONGITUDE: 110.111700 * DATE/TIME START: 1973-01-02T00:00:00 * DATE/TIME END: 1973-01-02T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.0 m * MAXIMUM DEPTH, sediment/rock: 375.0 m 1986-02-14 text/tab-separated-values, 162 data points https://doi.pangaea.de/10.1594/PANGAEA.757317 https://doi.org/10.1594/PANGAEA.757317 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.757317 https://doi.org/10.1594/PANGAEA.757317 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Sackett, William M (1986): d13C signatures of organic carbon in southern high latitude deep sea sediments; paleotemperature implications. Organic Geochemistry, 9(2), 63-68, https://doi.org/10.1016/0146-6380(86)90087-2 28-266 Antarctic Ocean/RIDGE Calcium carbonate Carbon organic total Deep Sea Drilling Project DEPTH sediment/rock DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Epoch Glomar Challenger Leg28 Sample code/label δ13C organic carbon Dataset 1986 ftpangaea https://doi.org/10.1594/PANGAEA.757317 https://doi.org/10.1016/0146-6380(86)90087-2 2023-01-20T08:51:58Z The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal that is traceable in deep-sea cores taken in high latitude regions of the Southern hemisphere. This signal may be weakened by noise due to (1) terrestrially derived debris in areas close to the continents; (2) changing current patterns resulting in varying settling trajectories; (3) erosion and redeposition and (4) maturation-diagenetic effects. Data for two cores taken southwest of Australia are evaluated with respect to these interferences. Dataset Antarc* Antarctic Antarctic Ocean PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Antarctic Ocean ENVELOPE(110.111700,110.111700,-56.402200,-56.402200)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 28-266
Antarctic Ocean/RIDGE
Calcium carbonate
Carbon
organic
total
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Epoch
Glomar Challenger
Leg28
Sample code/label
δ13C
organic carbon
spellingShingle 28-266
Antarctic Ocean/RIDGE
Calcium carbonate
Carbon
organic
total
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Epoch
Glomar Challenger
Leg28
Sample code/label
δ13C
organic carbon
Sackett, William M
Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266
topic_facet 28-266
Antarctic Ocean/RIDGE
Calcium carbonate
Carbon
organic
total
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Epoch
Glomar Challenger
Leg28
Sample code/label
δ13C
organic carbon
description The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal that is traceable in deep-sea cores taken in high latitude regions of the Southern hemisphere. This signal may be weakened by noise due to (1) terrestrially derived debris in areas close to the continents; (2) changing current patterns resulting in varying settling trajectories; (3) erosion and redeposition and (4) maturation-diagenetic effects. Data for two cores taken southwest of Australia are evaluated with respect to these interferences.
format Dataset
author Sackett, William M
author_facet Sackett, William M
author_sort Sackett, William M
title Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266
title_short Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266
title_full Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266
title_fullStr Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266
title_full_unstemmed Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266
title_sort concentration and stable carbon isotopic composition of organic carbon of dsdp hole 28-266
publisher PANGAEA
publishDate 1986
url https://doi.pangaea.de/10.1594/PANGAEA.757317
https://doi.org/10.1594/PANGAEA.757317
op_coverage LATITUDE: -56.402200 * LONGITUDE: 110.111700 * DATE/TIME START: 1973-01-02T00:00:00 * DATE/TIME END: 1973-01-02T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.0 m * MAXIMUM DEPTH, sediment/rock: 375.0 m
long_lat ENVELOPE(110.111700,110.111700,-56.402200,-56.402200)
geographic Antarctic
Antarctic Ocean
geographic_facet Antarctic
Antarctic Ocean
genre Antarc*
Antarctic
Antarctic Ocean
genre_facet Antarc*
Antarctic
Antarctic Ocean
op_source Supplement to: Sackett, William M (1986): d13C signatures of organic carbon in southern high latitude deep sea sediments; paleotemperature implications. Organic Geochemistry, 9(2), 63-68, https://doi.org/10.1016/0146-6380(86)90087-2
op_relation https://doi.pangaea.de/10.1594/PANGAEA.757317
https://doi.org/10.1594/PANGAEA.757317
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.757317
https://doi.org/10.1016/0146-6380(86)90087-2
_version_ 1766152355980509184

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